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Fig. 4.11 Two views of an ice-edge band observed during the 1983 MIZEX project in the Green-
land Sea from the bridge of theR/V Pol arbj orn
will most likely suffice most of the time. 3 Nevertheless,
the basic scaling ideas behind the relatively simple similarity theory described in
this chapter, particularly the buoyancy scaling factor,
neutral scaling
( η =
1
)
η , form the basis for more
complexmodelingoftheIOBLpresentedlater.Andthebasicpointbehindsimilarity
3 When the well mixed layer is shallow compared to the dynamic IOBL depth (nominally
0
.
4
η u 0 /
f )interaction withfluidinthepycnocline willmodify thedrag relation.
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